Japan Geoscience Union Meeting 2014

Presentation information

Oral

Symbol S (Solid Earth Sciences) » S-IT Science of the Earth's Interior & Techtonophysics

[S-IT38_30AM1] Rheology and Transport Phenomena of Geomaterials

Wed. Apr 30, 2014 9:00 AM - 10:45 AM 511 (5F)

Convener:*Tomohiro Ohuchi(Geodynamics Research Center, Ehime University), Osamu Kuwano(Japan Agency for Marin-Earth Science and Technology), Ichiko Shimizu(Department of Earth and Planetary Science, Graduate School of Science, University of Tokyo), Chair:Ichiko Shimizu(Department of Earth and Planetary Science, Graduate School of Science, University of Tokyo)

10:15 AM - 10:30 AM

[SIT38-06] New modelling devices to enhance the reproducibility of analogue model experiments

*Tatsuya DOTARE1, Yasuhiro YAMADA1, Hide SAKAGUCHI2, Takane HORI2 (1.Department of Urban Management, Kyoto University, 2.Japan Agency for Marine-Earth Science and Technology (JAMSTEC))

Keywords:analogue modelling, sandbox, reproducibility, accrationary prism, heterogeniety

The scaled analogue model experiments have been used for more than 100 years to reproduce the geological development processes in the laboratory scales using the granular material (e.g. dry sand). Recently, we can obtain the small-scale deformation quantitatively by applying digital image analyses. Then, we observed the 'weak shear band' before fault initiation process. However, heterogeneity in the initial model produced by human hand often causes the fluctuation of the experimental results (e.g. fault location, faulting timing and fault geometry). To solve this problem, we made the experimental device for making the initial model automatically and conducted the experiments to compare the experimental results with the previous method. We conducted simple convergent experiments. Initial models were made by previous method (human hand) or new method (new device) and experiments were repeated 5 times, respectively. As a result, while branches of new faults can be seen in the previous method, there are no branches in the new method. In addition, the fluctuation of experimental results was restricted in the new method.This shows that new experimental device can make the initial model homogeneous and reproduce the same initial model in each experiment.